Copy of Basic Map Reading

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    Map Reading

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      A Map is a birds eye view of thesurrounding area to help guide us

    from one place to another.

    What is a Map?

     A traveller needs a map to help

    them find their way aroundmore easily.

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    Lines of Longitude

    Lines of Longitude run parallel to the Prime

    Meridian at Greenwich.

     A line of

    Longitude is

    also referred toas a Meridian

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    Lines of Latitude

    • Lines of Latitude run parallel to the Equator

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    Recording your Position

    Lines of Latitude &Longitude cometogether to form amatrix

    1.5 

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    Recording your Position

    l First we state its

    Latitude followed

    by its Longitude

    in degrees &

    minutes

    e.g.:A= 20’N 56’W 

    B= 17’S 17’W 

    C= 45’N 15’E 

    1.5 

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      Although this system can give reasonably

    accurate positioning it is not accurate

    enough for everyday use.

    So each degree is further broken down

    into 60 minutes.

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    Topographical Maps

    This means they show the shape and surface

    detail of the land. This includes natural and

    man-made features.

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    Looking after your map

    Some maps are now produced laminated and you

    can treat maps with a waterproof coating

     Always keep your map folded

    NEVER mark a map surface with ink

    If you do need to mark your map do so lightly

    with a pencil

    Try to avoid getting it wet

    If you do get it wet allow it to dry naturally.

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    Folding your map

    First fold your map in half length wise, with theprinted map outwards like so:

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    Then concertinawise:

    The unit of height used on this map is in

    METRES.

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    Latitude / Longitude

    The lines of latitude are expressed in degrees

    and minutes and are marked along the right

    and left (east and west) hand side of the map.

    The lines of longitude are marked along the

    top and bottom (north and south). The lines

    of latitude and longitude are not actuallydrawn on the map itself - it would be too

    confusing.

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    North

    1. True North

    2. Grid North

    3. Magnetic north

    In map reading there are always references to

    north. There are in fact 3 north's:

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    True North

    This is the geographical north pole of the

    earth - the point where the earth’s axis meet

    the surface.

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    Grid North

    This north takes its name from the National GridSystem. This is a system of imaginary linesdrawn vertically & horizontally on the mapwhich divide it into a series of squares.

    Because Grid lines are drawn on a flat

    map and lines of latitude & longitude are

    curved like the earth's surface. The 2

    systems are different.

    This difference is shown on the map (key

    position 10) as a difference between True

    & Grid north.

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    Magnetic North

    This is the point the magnetic needle aligns

    itself to when freely suspended. The earth hasits own magnetic field.

    Unfortunately the earth’s  north and southpoles do not line up with the geographical poles

    - in fact they are about 1200 miles apart!!

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    Sometimes the same symbol is shown in

    different colours to signify a difference

    Example

    Red National Trust symbols show the area is

    open all year.

    The same symbol in blue indicates it has a

    restricted opening period.

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    Contour Lines

     A contour line is a reddish brown line drawn

    on the map joining all points of equal height

    above mean sea level (MSL) Mean sea level

    is a fixed height approximately half waybetween high and low tides.

    By joining all the pointsat the same height you

    can achieve a picture

    and shape of the land.

    50

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    These contour lines will wonder all over the

    map and will eventually rejoin at the startpoint to show an area of equal height.

    The only exception to this rule is where acontour line meets a cliff face.

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    The height is shown in small breaks in the

    contour line.

    Every 5th line is shown thicker to make themeasier to read.

    These contour lines are situated at 10 metre

    intervals.The rise & fall between contours is the Vertical

    Interval (VI)

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    Scales

    The objective of this lecture is foryou to be able to display an

    reasonable understanding of size and

    scale in map work.

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    IntroductionIf your map is to cover a reasonable area

    then everything on the map has to be

    reduced considerably from its real size.

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    Why do we use scale?

    We use scale so that we can cover a

    reasonable area of the ground aroundus and show it on the map.

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    How do you express scale?

    There are 3 ways to express

    scale.

    These are:

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    A: In Words

    B by saying “so many centimetres to the kilometre” 

    Example: a scale of “2cm to 1km” means

    that for every 2 cm on the map you would

    travel 1 km on the ground.

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    B: As a Representative Fraction

    In this method the scale is expressed in the

    form of a fraction.

    e.g. 1

    50,000

    Using this method you are saying that anydistances measured on the map are one-

    fiftythousanth of the real distance on the

    ground.

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    A Representative Fraction is

    also referred to as RF

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    C: As a Ratio

    This is very similar to B, but is written as:

    1:50,000

    this means the same as:

    1

    50,000

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    Calculation

    In the case of RF and ratio the expression of

    distance, whether it’s  inches, centimetres or

    metres, is the measurement on the ground

    l 1 inch on the map = 50,000 inches on the ground

    l 1 cm on the map = 50,000 cm on the ground

    l 1 m on the map = 50,000 m on the ground

    So a 1:50,000 ratio would be equally validfor:

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    If the scale is expressed in words it

    may be necessary to convert it intoeither a RF or a ratio.

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    For example: to convert a scale of 1 inch to

    1 mile, you have to calculate the number ofinches in a mile:

    •  There are 1,760 yards in a mile

    •  There are 5,280 feet in a mile (1760 x 3)

    •  There are 63,360 inches in a mile (5280 x

    12)

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    So the scale of 1 inch to 1 milecan be expressed as a ratio of

    1:63,360.

    This type of calculation is made

    easier using the metric system,

    but it will still require carefulthought.

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    Area

    When using scales, areas of ground

    will also be proportionately reduced

    but remember that areas contract

    rapidly on small scale maps.

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    For example if you take a map that is half the

    scale of another, then the area is reduced by

    a quarter (not a half). This is because thearea of a rectangular figure is length

    multiplied by breadth. If you therefore halved

    the scale you will quarter the area of themap.4

    4

    4 x 4 = 16

    2

    2

    2 x 2 = 4

    e.g.

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    The same area of ground in three different scales

    (Half the scale = One quarter of the area)

    1 km square

    at 1:12,500

    1 km squareat 1:25,000

    1 km square

    at 1:50,000

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    Examples of different scales:

    Large scale - City or town maps(defined buildings)

    Medium scale - Larger areas (buildings

    as symbols)

    Small scale - Atlas (large towns inname only)